
mineral
Tumbled blue chalcedony or pale aquamarine-like quartz
Chalcedony (microcrystalline SiO₂), possibly blue quartz; visual identification is uncertain
AI-generated identification · may be incorrectTranslucent blue-gray to colorless, vitreous/waxy luster, no visible cleavage, conchoidal fracture, and likely Mohs hardness about 6.5–7; rounded edges indicate tumbling or polishing.
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Physical properties
Translucent blue-gray to colorless, vitreous/waxy luster, no visible cleavage, conchoidal fracture, and likely Mohs hardness about 6.5–7; rounded edges indicate tumbling or polishing.
Formation & geological history
Quartz-rich silica formed from hydrothermal or groundwater fluids in cavities and fractures; chalcedony commonly formed during the Cenozoic, though its exact age cannot be determined visually.
Uses & applications
Used as a decorative tumbled stone, cabochon, carving material, and collector specimen; quality blue chalcedony may be used in jewelry.
Geological facts
The cloudy internal wisps and smooth polish are consistent with chalcedony, but the image alone cannot exclude glass or another quartz variety. Natural chalcedony commonly shows subtle fibrous translucency rather than distinct large crystals.
Field identification & locations
Test with a steel file or quartz point: genuine quartz should resist scratching; glass may show bubbles and scratches more readily. Common sources include Brazil, India, Madagascar, Turkey, and the United States.
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